Fabio Arzilli
Dendritic crystallization in hydrous basaltic magmas controls magma mobility within the Earth’s crust
Arzilli, Fabio; Polacci, Margherita; La Spina, Giuseppe; Le Gall, Nolwenn; Llewellin, Edward W.; Brooker, Richard A.; Torres-Orozco, Rafael; Di Genova, Danilo; Neave, David A.; Hartley, Margaret E.; Mader, Heidy M.; Giordano, Daniele; Atwood, Robert; Lee, Peter D.; Heidelbach, Florian; Burton, Mike R.
Authors
Margherita Polacci
Giuseppe La Spina
Nolwenn Le Gall
Professor Edward Llewellin ed.llewellin@durham.ac.uk
Professor
Richard A. Brooker
Rafael Torres-Orozco
Danilo Di Genova
David A. Neave
Margaret E. Hartley
Heidy M. Mader
Daniele Giordano
Robert Atwood
Peter D. Lee
Florian Heidelbach
Mike R. Burton
Abstract
The majority of basaltic magmas stall in the Earth’s crust as a result of the rheological evolution caused by crystallization during transport. However, the relationships between crystallinity, rheology and eruptibility remain uncertain because it is difficult to observe dynamic magma crystallization in real time. Here, we present in-situ 4D data for crystal growth kinetics and the textural evolution of pyroxene during crystallization of trachybasaltic magmas in high-temperature experiments under water-saturated conditions at crustal pressures. We observe dendritic growth of pyroxene on initially euhedral cores, and a surprisingly rapid increase in crystal fraction and aspect ratio at undercooling ≥30 °C. Rapid dendritic crystallization favours a rheological transition from Newtonian to non-Newtonian behaviour within minutes. We use a numerical model to quantify the impact of rapid dendritic crystallization on basaltic dike propagation, and demonstrate its dramatic effect on magma mobility and eruptibility. Our results provide insights into the processes that control whether intrusions lead to eruption or not.
Citation
Arzilli, F., Polacci, M., La Spina, G., Le Gall, N., Llewellin, E. W., Brooker, R. A., Torres-Orozco, R., Di Genova, D., Neave, D. A., Hartley, M. E., Mader, H. M., Giordano, D., Atwood, R., Lee, P. D., Heidelbach, F., & Burton, M. R. (2022). Dendritic crystallization in hydrous basaltic magmas controls magma mobility within the Earth’s crust. Nature Communications, 13(1), https://doi.org/10.1038/s41467-022-30890-8
Journal Article Type | Article |
---|---|
Acceptance Date | May 13, 2022 |
Online Publication Date | Jun 10, 2022 |
Publication Date | 2022 |
Deposit Date | Jul 19, 2022 |
Publicly Available Date | Jul 19, 2022 |
Journal | Nature Communications |
Publisher | Nature Research |
Peer Reviewed | Peer Reviewed |
Volume | 13 |
Issue | 1 |
DOI | https://doi.org/10.1038/s41467-022-30890-8 |
Public URL | https://durham-repository.worktribe.com/output/1197228 |
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This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
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